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References
geochemsitry of organic matter and minerals during
diagenesis and hydrocarbon migration. Geochimica
et Cosmochimica Acta 59: 765-779.
Wu, G., Berger, W.H., 1989. Planktonic foraminifera:
differential dissolution and the Quaternary stable
isotope record in the west Equatorial Pacific.
Paleoceanography 4: 181-198.
Zahn, R., Keir, R., 1994. Tracer-nutrient correlations in
the upper ocean: observational and box model
constraints on the use of benthic foraminiferal δ
13 C
and Cd/Ca as paleo-proxies for the intermediatedepth ocean. In: Zahn, R., Pedersen, T.F., Kaminski,
M.A., Labeyrie, L., (eds), Carbon cycling in the
glacial ocean: Constraints on the ocean’s role in
global change. Springer, Berlin, pp 195-223.
Zahn, R., Mix, A.C., 1991. Benthic foraminiferal δ
18 O in
the ocean’s temperature-salinity-density field: Constraints on ice age thermohaline circulation. Paleoceanography 6: 1-20.
Zeebe, R.E., Wolf-Gladrow, D.A., Bijma, J., Hšnisch, B.,
2003. Vital effects in foraminifera do not compromise the use of d
11 B as a paleo-pH indicator:
Evidence from modeling. Paleoceanography 18: PA
1 0 4 3 .
Zeebe, R.E., and Sanyal, A., 2002. Comparison of two
potential strategies of planktonic foraminifera for
house building: Mg
2+ or H
+ removal? Geochim.
Cosmochim. Acta, 66: 1159-1169.
Zeebe, R.E., 1999. An explanation of the effect of
seawater carbonate concentration on foraminiferal
oxygen isotopes. Geochimica et Cosmochimica Acta
63: 2001-2007.
Zeebe, R.E., 2001. Seawater pH and isotopic paleotemperatures of Cretaceous oceans. Palaeogeography, Palaeoclimatology, Palaeoecology, 170:49-57.
References
geochemsitry of organic matter and minerals during
diagenesis and hydrocarbon migration. Geochimica
et Cosmochimica Acta 59: 765-779.
Wu, G., Berger, W.H., 1989. Planktonic foraminifera:
differential dissolution and the Quaternary stable
isotope record in the west Equatorial Pacific.
Paleoceanography 4: 181-198.
Zahn, R., Keir, R., 1994. Tracer-nutrient correlations in
the upper ocean: observational and box model
constraints on the use of benthic foraminiferal δ
13 C
and Cd/Ca as paleo-proxies for the intermediatedepth ocean. In: Zahn, R., Pedersen, T.F., Kaminski,
M.A., Labeyrie, L., (eds), Carbon cycling in the
glacial ocean: Constraints on the ocean’s role in
global change. Springer, Berlin, pp 195-223.
Zahn, R., Mix, A.C., 1991. Benthic foraminiferal δ
18 O in
the ocean’s temperature-salinity-density field: Constraints on ice age thermohaline circulation. Paleoceanography 6: 1-20.
Zeebe, R.E., Wolf-Gladrow, D.A., Bijma, J., Hšnisch, B.,
2003. Vital effects in foraminifera do not compromise the use of d
11 B as a paleo-pH indicator:
Evidence from modeling. Paleoceanography 18: PA
1 0 4 3 .
Zeebe, R.E., and Sanyal, A., 2002. Comparison of two
potential strategies of planktonic foraminifera for
house building: Mg
2+ or H
+ removal? Geochim.
Cosmochim. Acta, 66: 1159-1169.
Zeebe, R.E., 1999. An explanation of the effect of
seawater carbonate concentration on foraminiferal
oxygen isotopes. Geochimica et Cosmochimica Acta
63: 2001-2007.
Zeebe, R.E., 2001. Seawater pH and isotopic paleotemperatures of Cretaceous oceans. Palaeogeography, Palaeoclimatology, Palaeoecology, 170:49-57.